Abstract
Glaciers and snow are the very symbol of the Arctic, covering large parts of its terrestrial surface throughout the year. The cool temperatures that have allowed for the widespread coverage of glaciers are now trending towards a warmer climate, and with this gradual shift we observe an abrupt response in the cryosphere of which glaciers are a key component. This change is manifested in retreating fronts and an overall thinning. Because the typology of Arctic glaciers is rich and varied, the response pattern to the on-going warming is not unison. Instead, there are large spatial variations due to the critical balance between summer temperature and winter precipitation in addition to other factors such as aspect, altitude, geographical location, debris cover, calving and so forth. Still, minor variations is superimposed on a larger trends which suggests that in a not so distant future, glaciers will probably be less abundant than what has been common for the last 100 years. In the context of the last 10,000 years it is evident that arctic glaciers have changed significantly and they have even been smaller than they are today, which was the case 9,000 to 5,000 years ago. On Svalbard, two glacier lake sediment records foretell of large past variations, indicating a more articulated sensitivity to climate change than what is commonly perceived for the Arctic cryosphere.
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Acknowledgement
We are very grateful that John Inge Svendsen kindly offered additional analysis to be conducted on core (#6) initially retrieved from Lake Linné. We thank the reviewer (Ann Hormes) for valuable and constructive criticism. This work is written in memory of the late Prof. Reidar Løvlie, who worked on a number of polar sediment archives on Svalbard, and was initially part of this effort.
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Paasche, Ø., Bakke, J. (2015). The Fleeting Glaciers of the Arctic. In: Evengård, B., Nymand Larsen, J., Paasche, Ø. (eds) The New Arctic. Springer, Cham. https://doi.org/10.1007/978-3-319-17602-4_7
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DOI: https://doi.org/10.1007/978-3-319-17602-4_7
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